El propósito de este documento es compartir una visión estratégica para mejorar la resiliencia costera en la región de San Diego-Baja California a través de la colaboración binacional basada en una evaluación de necesidades liderada por California Sea Grant y Climate Science Alliance.La visión de este documento identifica oportunidades clave y estrategias accionables que integran la investigación científica, el conocimiento tradicional y prácticas innovadoras para apoyar a las comunidades y ecosistemas costeros. Al fomentar asociaciones transfronterizas, expandir las capacidades de investigación y comprometer a diversos actores, este documento tiene como objetivo guiar los esfuerzos hacia un futuro más resiliente para nuestra costa compartida.

The purpose of this document is to outline a strategic vision for enhancing coastal resilience in the San Diego-Baja California Region through binational collaboration. It draws from a needs assessment led by California Sea Grant and the Climate Science Alliance. This vision document identifies key opportunities and actionable strategies that integrate scientific research, traditional knowledge, and innovative practices to support resilient coastal communities and ecosystems. By fostering cross-border partnerships, expanding research capabilities, and engaging diverse stakeholders, this document aims to guide efforts towards a more resilient future for our shared coastline.

Recent climate-change research largely confirms the impacts on US ecosystems identified in the 2009 National Climate Assessment and provides greater mechanistic understanding and geographic specificity for those impacts. Pervasive climate-change impacts on ecosystems are those that affect productivity of ecosystems or their ability to process chemical elements. Loss of sea ice, rapid warming, and higher organic inputs affect marine and lake productivity, while combined impacts of wildfire and insect outbreaks decrease forest productivity, mostly in the arid and semi-arid West. Forests in wetter regions are more productive owing to warming. Shifts in species ranges are so extensive that by 2100 they may alter biome composition across 5-20% of US land area. Accelerated losses of nutrients from terrestrial ecosystems to receiving waters are caused by both winter warming and intensification of the hydrologic cycle. Ecosystem feedbacks, especially those associated with release of carbon dioxide and methane release from wetlands and thawing permafrost soils, magnify the rate of climate change. © The Ecological Society of America.